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  • 1
    Publication Date: 2024-02-15
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Snow petrels (〈italic〉Pagodroma nivea〈/italic〉), which are endemic to the Antarctic region, produce proventricular stomach oil from ingested food for feeding purposes but also spit the oil in the immediate surrounds of the nests, where it forms encrustations over time (Antarctic mumiyo). These deposits provide a unique opportunity to understand the paleo‐ecological diet of snow petrels and because the seabirds forage in the ocean, they potentially provide an archive of past marine environmental conditions in the Southern Ocean. For validating methods for reconstructions we use compositional data obtained on modern stomach oils and DNA data from fecal samples of snow petrels. We find that the distribution of carboxylic acid compounds in modern stomach oils and in the fossil deposits are consistent with variable contributions of fish and krill, which are the main constituents of modern snow petrel diet, and allows inference of past changes in snow petrel diet from the fossil record. Analyses of mumiyo deposits from six regions in East Antarctica reveal systematic differences in the isotopic composition of organic matter (δ〈sup〉13〈/sup〉C and δ〈sup〉15〈/sup〉N) and carboxylic acid patterns. This may suggest regional and/or temporal variability in the composition of snow petrels diet, likely differing in response to the prevailing environmental conditions in the foraging range of the birds, such as sea‐ice variability, polynya activity and primary productivity. Our study provides confidence for using these approaches for broader scale paleo‐studies in the future and for an assessment of the temporal changes and regional variability in snow petrel diet.〈/p〉
    Description: Plain Language Summary: To better understand interactions of biological and physical processes in Antarctic marine ecosystems, we investigate fossil deposits of stomach oil of snow petrels for their use as a geological archive for past environmental changes. The deposits form over time in the surroundings of the nesting cavities of snow petrels, which produce stomach oil from ingested food but also spit it at nest robbers. In fresh oil the lipid and isotopic composition can be traced back to the composition of snow petrel food, such as variable proportions of fish and krill. From comparing the lipid and δ〈sup〉13〈/sup〉C‐isotopic composition of modern oil to fossil deposits we suggest it is possible to identify changes in the diet of snow petrels in the fossil record. Since the composition of the diet is closely linked to the prevailing environmental conditions in the marine foraging region of the birds, such as summer sea ice extent, this information can be used for paleoenvironmental reconstructions. Our study of deposits from widely separated regions in Antarctica shows that there are spatial and temporal differences in the composition of stomach oil deposits, likely related to the prevailing environmental conditions. This finding underpins the application of our approach.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Modern stomach oil and feces of snow petrels are used to validate paleo‐proxies for environmental reconstructions in East Antarctica〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Biomarkers and isotopic composition of fossil stomach oil deposits of snow petrels reflect past composition in diet〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Changes in the composition of the paleo‐ecological diet reflect variations of environmental conditions in the coastal Southern Ocean〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Description: Australian Antarctic Division http://dx.doi.org/10.13039/501100005108
    Description: https://doi.org/10.1594/PANGAEA.951357
    Keywords: ddc:560 ; Antarctica ; paleoclimate ; sea ice ; fatty acids ; stable isotopes ; stomach oil deposits
    Language: English
    Type: doc-type:article
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 315 (1985), S. 131-133 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Fig. 1 Sketch map of the working area with locations mentioned in the text. The arrows show the main glacier flows feeding Lake Untersee. L.U., Lake Untersee; L.O., Lake Obersee; S.P., sampling point. On the northeastern margin of the mountains in central Dron-ning Maud Land, pilots of the German ...
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2019-01-01
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
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  • 4
    Publication Date: 1985-05-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 5
    Publication Date: 1988-01-01
    Description: Since 1978 scientists from the German Democratic Republic, in collaboration with members of Soviet Antarctic Expeditions, have been studying the isotopic composition of ice and snow, as well as the trapped gas content of glacier ice from northern Queen Maud Land near 12 °E, in order to decipher recent structures and Holocene evolution of this part of the margin of the East Antarctic ice sheet.Along a 180 km north-south profile three large bodies could be distinguished: (1) Novolazarevskaya Ice Shelf (100 km wide, ≲700 m thick); (2) the ice cover (30 km wide, ≲300 m thick) of the Skaly Instituta Geologii Arktiki nunataks [“Skaly IGA”], with a scarp to the Schirmacher oasis; and (3) a firn glacier (50 km wide, c. 1000 m thick), filling the depression between “lskaly IGA” and the Wohlthat massif.The ice-flow conditions of the surface layer are known. On the basis of isotope profiles from Soviet drilling sites on the ice shelf (447 m core) and on the firn glacier (809 m core), from the scarp and slope of the inland ice to the south of the Schirmacher oasis (ablation zone), and from numerous pits through the surface layer, a preliminary stratigraphic model has been developed.On the basis of recent flow conditions, the basal layer of Novolazarevskaya Ice Shelf and that of the inland ice of the “Skaly IGA” region were identified as relics of late Pleistocene ice cover by their mean deuterium content of −390 and −330% respectively. The old ice is covered by Holocene layers of regional origin (δD = −230 to −150%); in the ice shelf there are also layers derived from the interior of Antarctica (δD = −350 to −280%).The isotope profile of the firn glacier (range of δ18O variations −32.3 to −18.1%, identifiable annual layers of about 20 cm of ice to a depth of 500 m) represents a unique record of the last 7–8 ka for this region. It is also supported by measurements of the total air content trapped in ice samples (V = 107–127 cm3/kg) taken from the 809 m core. Details will be published elsewhere.More information is expected to be provided by isotope studies of extended blue-ice fields and ice-cored moraines.
    Print ISSN: 0260-3055
    Electronic ISSN: 1727-5644
    Topics: Geography , Geosciences
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  • 6
    Publication Date: 1988-01-01
    Description: Since 1978 scientists from the German Democratic Republic, in collaboration with members of Soviet Antarctic Expeditions, have been studying the isotopic composition of ice and snow, as well as the trapped gas content of glacier ice from northern Queen Maud Land near 12 °E, in order to decipher recent structures and Holocene evolution of this part of the margin of the East Antarctic ice sheet. Along a 180 km north-south profile three large bodies could be distinguished: (1) Novolazarevskaya Ice Shelf (100 km wide, ≲700 m thick); (2) the ice cover (30 km wide, ≲300 m thick) of the Skaly Instituta Geologii Arktiki nunataks [“Skaly IGA”], with a scarp to the Schirmacher oasis; and (3) a firn glacier (50 km wide, c. 1000 m thick), filling the depression between “lskaly IGA” and the Wohlthat massif. The ice-flow conditions of the surface layer are known. On the basis of isotope profiles from Soviet drilling sites on the ice shelf (447 m core) and on the firn glacier (809 m core), from the scarp and slope of the inland ice to the south of the Schirmacher oasis (ablation zone), and from numerous pits through the surface layer, a preliminary stratigraphic model has been developed. On the basis of recent flow conditions, the basal layer of Novolazarevskaya Ice Shelf and that of the inland ice of the “Skaly IGA” region were identified as relics of late Pleistocene ice cover by their mean deuterium content of −390 and −330% respectively. The old ice is covered by Holocene layers of regional origin (δD = −230 to −150%); in the ice shelf there are also layers derived from the interior of Antarctica (δD = −350 to −280%). The isotope profile of the firn glacier (range of δ18O variations −32.3 to −18.1%, identifiable annual layers of about 20 cm of ice to a depth of 500 m) represents a unique record of the last 7–8 ka for this region. It is also supported by measurements of the total air content trapped in ice samples (V = 107–127 cm3/kg) taken from the 809 m core. Details will be published elsewhere. More information is expected to be provided by isotope studies of extended blue-ice fields and ice-cored moraines.
    Print ISSN: 0260-3055
    Electronic ISSN: 1727-5644
    Topics: Geography , Geosciences
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